the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A Pan-Arctic Pigment Database for Phytoplankton and Sea-Ice Algae
Abstract. Climate change has dramatically altered the Arctic seas with significant decrease in sea ice extent and thickness and warming water temperature. The ecological impacts of such change have been described for many parts of the Arctic Ocean, but long-term records of biological indicators are still missing. Among those, photosynthetic and accessory pigments are one of the key tools that aid quantification of phytoplankton and sea-ice algae biomass and characterisation of community composition. To address this gap, we present the first pan-Arctic compilation of in situ algal pigment data obtained exclusively by High-Performance Liquid Chromatography (HPLC), containing 10.798 samples collected across 77 Arctic research cruises between 2000 and 2024. As a result of large-scale collaborative effort, this database covers both open water and sea-ice environments across coastal, shelf and open domains. The database (10.11583/DTU.29445104) includes measures of up to 26 pigments, with 8 major marker/accessory pigments being considered in this study, namely Alloxanthin (Allo), 19’-Butanoyloxyfucoxanthin (Butfuco), Chlorophyll a (Chl-a), Chlorophyll b (Chl-b), Fucoxanthin (Fuco), 19’-Hexanoyloxyfucoxanthin (Hexfuco), Peridinin (Peri), and Zeaxanthin (Zea). This publicly available database provides crucial data that can be used to assess phytoplankton dynamics, validating remote sensing observations and can serve as a resource for future Arctic ecological- and modelling studies.
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Status: open (until 18 May 2026)
- RC1: 'Comment on essd-2026-144', Anonymous Referee #1, 21 Apr 2026 reply
Data sets
Consolidated Arctic Pigments (2000-2024) Heidemann et al. https://doi.org/10.11583/DTU.29445104
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General comments
The authors compiled phytoplankton/ice algae pigment concentration data obtained from numerous cruises in the Arctic Ocean. The dataset encompasses the concentrations of chlorophylls and accessory pigments, which are beneficial for estimating phytoplankton community structure and validating ocean color sensors.
While the dataset is highly valuable, the investigation of data quality was limited to categorization based on the availability of pigments and metadata. Methods for HPLC measurement, such as those employed by Zapata et al. (2000) and Van Heukelem and Thomas (2001), as well as the HPLC system, solvent, extraction techniques, and other relevant information are criteria to compare concentrations from different laboratories. The author wrote these variations as uncertainties. Therefore, users have to trace original dataset or articles to know them. Although round-robin experiments have been conducted to compare results from different laboratories, not all laboratories participated in the experiments. Additionally, the sampling technique and measurement methods for ice algae pigments are not explicitly mentioned. I acknowledge the data correction among laboratories is challenging and I believe that the pigment concentrations in this dataset were analyzed using reliable methodologies. However, providing information on the methods employed by the data provider is beneficial for conducting further data analyses. In summary, the dataset presented in this paper is suitable for publication in ESSD after minor revisions of the manuscript and dataset.
Specific comments
Through the manuscript, "a", "b", and "c" of chlorophylls are sometime not italicized. Pigment names were repeatedly abbreviated. Please check them.
L121-122: Absorption and scattering coefficients of phytoplankton are estimated from reflectance. They are not directly detected by radiometers.
Table 1: What are Dinoflagellates-1 and 2?
Table 1: Chl-c1+c2: MgDVP has very close retention time to chl-c1 and c2. All laboratories measured as only c1+c2?
L155: Hayward et al. (2025)? The paper in 2024 is study in the Southern Ocean.